{"id":64,"date":"2024-02-10T01:29:20","date_gmt":"2024-02-10T06:29:20","guid":{"rendered":"http:\/\/localhost\/wordpress\/?page_id=64"},"modified":"2024-08-24T16:07:50","modified_gmt":"2024-08-24T14:07:50","slug":"roc","status":"publish","type":"page","link":"https:\/\/hydrogeomtl.com\/?page_id=64","title":{"rendered":"G\u00e9ologie du roc"},"content":{"rendered":"\n

Une partie des eaux souterraines s’\u00e9coule dans les fractures du roc de l’\u00eele de Montr\u00e9al. Cet aquif\u00e8re est confin\u00e9 lorsqu’il se situe sous des couches argileuses.<\/p>\n\n\n\n

Carte g\u00e9ologique des Basses-Terres-du-St-Laurent, secteur de l’\u00eele de Montr\u00e9al :<\/h5>\n\n\n\n
\"\"<\/figure>\n\n\n\n
Carte de la topographie du roc de l’\u00eele de Montr\u00e9al au-dessus du Niveau Moyen de la Mer (N.M.M.) :<\/h5>\n\n\n\n
\"\"<\/figure>\n\n\n\n

La Topographie du roc (TR) est \u00e9gale au Mod\u00e8le Num\u00e9rique de Terrain (MNT) moins l’\u00c9paisseur des D\u00e9p\u00f4ts Meubles (EDM).<\/p>\n\n\n\n

Coupe g\u00e9ologique du roc de l’\u00eele de Montr\u00e9al :<\/h5>\n\n\n\n
\"\"<\/figure>\n\n\n\n

T\u00e9l\u00e9chargez ces cartes<\/h3>\n\n\n\n

Carte des Basses-Terres-du-St-Laurent :<\/p>\n\n\n\n

   Format Geopackage (.gpkg)<\/a><\/p>\n\n\n\n

   Format Google Earth (.kmz)<\/a><\/p>\n\n\n\n

Topographie du roc (TR) :<\/p>\n\n\n\n

   Format GeoTIFF (.tif)<\/a><\/p>\n\n\n\n

Source :<\/p>\n\n\n\n

   G\u00e9ologie des Basses-Terres-du-St-Laurent (Th\u00e9riault, 2014)<\/a><\/p>\n\n\n\n

   G\u00e9ologie des Basses-Terres-du-Saint-Laurent (Globensky, 1987)<\/a><\/p>\n\n\n\n

   Rapport g\u00e9ologique \u2013 R\u00e9gion de Montr\u00e9al (Clark, 1972)<\/a><\/p>\n\n\n\n

   Rapport pr\u00e9liminaire sur la r\u00e9gion de Montr\u00e9al (Clark, A.-O. Dufresne, 1941)<\/a><\/p>\n\n\n\n

   Mod\u00e9lisation g\u00e9ologique 3D du bassin des Basses-Terres du Saint-Laurent (B\u00e9dard, 2013)<\/a><\/p>\n\n\n\n

   G\u00e9ologie du Qu\u00e9bec (Hocq, 1994)<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

Une partie des eaux souterraines s’\u00e9coule dans les fractures du roc de l’\u00eele de Montr\u00e9al. Cet aquif\u00e8re est confin\u00e9 lorsqu’il se situe sous des couches argileuses. Carte g\u00e9ologique des Basses-Terres-du-St-Laurent, secteur de l’\u00eele de Montr\u00e9al : Carte de la topographie du roc de l’\u00eele de Montr\u00e9al au-dessus du Niveau Moyen de la Mer (N.M.M.) : […]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-64","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/hydrogeomtl.com\/index.php?rest_route=\/wp\/v2\/pages\/64","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/hydrogeomtl.com\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/hydrogeomtl.com\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/hydrogeomtl.com\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/hydrogeomtl.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=64"}],"version-history":[{"count":9,"href":"https:\/\/hydrogeomtl.com\/index.php?rest_route=\/wp\/v2\/pages\/64\/revisions"}],"predecessor-version":[{"id":379,"href":"https:\/\/hydrogeomtl.com\/index.php?rest_route=\/wp\/v2\/pages\/64\/revisions\/379"}],"wp:attachment":[{"href":"https:\/\/hydrogeomtl.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=64"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}